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Aquatic Vegetation in Relation to Soils
Author(s) -
Veatch J. O.
Publication year - 1932
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj1932.036159950b1320010003x
Subject(s) - citation , relation (database) , vegetation (pathology) , computer science , state (computer science) , library science , environmental science , data mining , medicine , algorithm , pathology
The ideal mineral eoil may be conc t ived as representing a certain balance, in the gross components: (1) solid matter (inorganic and organic) , (2) liquid mat ter , (3) gaseous ma t t e r . Departures from this ideal soil occur to such an ex t en t tha t the organic matter greatly dominates over the inorganic be in muck and peat soils, or the liquid) gaseous , and o r g a n i c parts may be email in relation to the inorganic part as in outcrops of geological formatione or hard rock s u r f a c e s . Again, tne liquid, or water part, may dominate as on permanently or pe r iod ica l ly wate r -covered surface such as lakes streams, and marshes. The conception of water soil (which might be designated as hydrosols or Hydrozome) and a suggestive plan of classif icat ion is p resen ted on to a accompanying chart.